| Display title | Physics:Condensation cloud |
| Default sort key | Condensation cloud |
| Page length (in bytes) | 5,510 |
| Namespace ID | 3020 |
| Namespace | Physics |
| Page ID | 403968 |
| Page content language | en - English |
| Page content model | wikitext |
| Indexing by robots | Allowed |
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| Counted as a content page | Yes |
| Page image |  |
| HandWiki item ID | None |
| Edit | Allow all users (infinite) |
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| Page creator | imported>QCDvac |
| Date of page creation | 05:44, 5 February 2024 |
| Latest editor | imported>QCDvac |
| Date of latest edit | 05:44, 5 February 2024 |
| Total number of edits | 1 |
| Recent number of edits (within past 90 days) | 0 |
| Recent number of distinct authors | 0 |
Description | Content |
Article description: (description)
This attribute controls the content of the description and og:description elements. | A transient condensation cloud, also called a Wilson cloud, is observable surrounding large explosions in humid air.
When a nuclear weapon or a large amount of a conventional explosive is detonated in sufficiently humid air, the "negative phase" of the shock wave causes a rarefaction of the air surrounding... |
